Results 161 to 170 of about 4,682,388 (200)
The 2025 M<sub>w</sub>7.7 Mandalay, Myanmar, earthquake reveals a complex earthquake cycle with clustering and variable segmentation on the Sagaing Fault. [PDF]
Antoine SL +7 more
europepmc +1 more source
Deceleration-phase restrengthening in compositionally zoned fault materials under transient slip. [PDF]
Woo S, Cheon Y, Han R, Lee H, Son M.
europepmc +1 more source
A dataset of hydrological effects induced by historical and modern earthquakes in Southern Apennines (Italy). [PDF]
Cucci L, Castellano C, Tertulliani A.
europepmc +1 more source
Coseismic crustal seismic velocity changes associated with the 2024 Mw 7.5 Noto earthquake, Japan
Paris N +11 more
europepmc +1 more source
An Mw 6.8 earthquake occurred in Luding County, Ganzi Tibetan Autonomous Prefecture, Sichuan Province, on 5 September 2022. This seismic event triggered numerous coseismic geohazards in the seismic zone. In this study, the ascending- and descending-track synthetic aperture radar (SAR) images observed by the Sentinel-1A satellite are utilized to extract
Yinghui Yang, Yiling Lu
exaly +5 more sources
Geometric complexities of a fault system have a significant impact on the rupture behavior of the fault. The 2021 Mw7.4 Maduo earthquake occurred on a multi-segmented complex sinistral fault in the interior of the Bayan-Har block in the northern Tibetan Plateau.
Jing Liu-Zeng
exaly +4 more sources
At 02:04 on May 22, 2021, an MS 7.4 earthquake occurred in Madoi County in Qinghai Province, China. This earthquake is the largest seismic event in China since the 2008 MS 8.0 Wenchuan earthquake. Thus, it is critical to investigate surface deformation and damage in time to accurately understand the seismogenic structure of the Madoi earthquake and the
Da Zhang, Yueren Xu, Ruoyu Mu
exaly +3 more sources
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Tectonophysics, 2021
Abstract Coseismic changes in slip direction recorded by curved slickenlines on fault surfaces are commonly observed following surface-breaking earthquakes. Such observations represent a dynamic record of seismic slip and may provide a new set of constraints on the evolution of propagating rupture and hence earthquake dynamics.
Clarrie Macklin +2 more
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Abstract Coseismic changes in slip direction recorded by curved slickenlines on fault surfaces are commonly observed following surface-breaking earthquakes. Such observations represent a dynamic record of seismic slip and may provide a new set of constraints on the evolution of propagating rupture and hence earthquake dynamics.
Clarrie Macklin +2 more
openaire +1 more source
Russian Geology and Geophysics, 2021
A 48 km long zone of surface deformation produced by the Ms = 7.3 intracontinental earthquake of 2003 in Gorny Altai is studied in its five segments between the Aktru and Irbistu rivers, where ruptures show the greatest offsets and distinct structural patterns.
E.M. Vysotsky +4 more
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A 48 km long zone of surface deformation produced by the Ms = 7.3 intracontinental earthquake of 2003 in Gorny Altai is studied in its five segments between the Aktru and Irbistu rivers, where ruptures show the greatest offsets and distinct structural patterns.
E.M. Vysotsky +4 more
openaire +1 more source
We estimate coseismic offsets at 20 sites in India due to the 25 April 2015 Gorkha, Nepal (Mw 7.8) earthquake. Only four sites in the Indian region, immediately to the south of the rupture, showed discernible coseismic horizontal offsets ranging between ...
Rajeev Kumar Yadav +2 more
exaly +2 more sources

